by Jeffrey C. Reid*; Kenneth B. Taylor*; Robert Mensah-Biney**; Jonathan Simms**, and Hamid Akbari***North Carolina Geological Survey **Minerals Research Laboratory, NC State University, Asheville, NC

AbstractThe Tungsten (Hamme) Queen mine is located at Tungsten, NC, 16 miles northwest of Henderson, NC, and 2 miles south of the

Virginia state line. The ore occurs in a near vertical quartz vein ranging in width from a few inches to several ft. Hübnerite, the

principal tungsten mineral, is accompanied by a minor amount of scheelite. Pyrite, the predominate metallic mineral in the

quartz veins, is accompanied by subordinate chalcopyrite, galena, sphalerite, and tetrahedrite. Fluorite is a common accessory

mineral in the ore and tailings.

Our objective was a preliminary evaluation to produce a high quality quartz concentrate from the approximately 2 million tons

of tailings present. Shallow drilling and pits <6 ft deep recovered ~60-pounds of wet tailings from gridded sites on the tailings

fan from just below the mill discharge point.

The quartz concentrate was produced using bench scale beneficiation methods including flotation, magnetic, and gravity sepa-

ration. Size fractions were evaluated for full mineral liberation and non-quartz species using binocular and petrographic micro-

scopes. Quartz analyses were obtained by ICP mass-spectrometry. A concentration flow chart was developed for the heavy and

light specific gravity fractions.

Chemical analysis indicates that the quartz may be suitable for fused quartz and silica glass applications. Fluorite comprises up

to ~2.5 wt. % of the heavy fraction and is a potential glass flux and other uses. Accessory hübnerite, scheelite, galena, chalcopy-

rite, and sphalerite may also be recoverable.

Study objectives

A high purity quartz concentrate was produced using bench scale beneficiation methods including flotation, magnetic, and gravity

separation.

Chemical analysis indicates that the quartz may be suitable for fused quartz and silica glass applications. Fluorite comprises up to

~2.5 wt. % of the heavy fraction and is a potential glass flux and other uses. Accessory hüebnerite, scheelite, galena, chalcopyrite,

and sphalerite may also be recoverable.

SEM-EDS

Tungsten Queen Mine Tailings Evaluation, Vance Co., NC: A Potential Silica Resource

Base Map: Geologic Map of the United States

(adapted from Schruben,

200 m

iso

bath

800 m

iso

bath

Mobil #3

Mobil #3

7Li 23Na 24Mg 27Al 39K 44Ca 47Ti 52Cr 55Mn 57Fe 60Ni 65Cu 66Zn 90Zr

0.884 3.774 2.809 35.47 12.53 76.98 6.695 0.033 1.789 13.26 0.023 1.52 1.485 0.085

Application SiO2 Other Elements Market Size Typical Price

Minimum (%) Maximum (%) Maximum

(ppm)

Mtpa US$/tonne

Clear glass

grade (fibers

and ceramics)

99.5 0.5 5,000 >70 30.00

Semiconductor

filler, LCD, and

optical glass

99.8 0.2 2,000 2 150.00

“Low grade”

HPQ

99.95 0.05 500 0.75 300.00

“Medium

grade” HPQ

99.99 0.01 100 0.25 500.00

“High grade”

HPQ

99.997 0.003 30 <0.1 >5,000

Suggested citation: Reid, Jeffrey C.; Taylor, Kenneth B.; Mensah-Biney, Robert; Simms, Jonathan, and Akbari, Hamid, 2017,

“Tungsten Queen Mine tailings evaluation, Vance Co., NC: A potential silica resource: North Carolina Geological Survey,

Open-file report 2017-01.

.

Summary and conclusions

Jae Ahn of The Quartz Corp. graciously provided us preliminary quartz concentrate analyses

as well as the quartz analysis presented here.

Sample collection

Analytical results

Petrography of fractions

This white concentrate color of the leached quartz (left) is contrasted

to the unleached concentrate(right). This is because the iron content

(a serious impurity) was greatly reduced by the leaching process.

Analytical results (ppm) of the leached quartz concentrate follow. Analysis was by ICP-MS. References and suggested readings

Acknowledgements

Bird, M. L. and Gair, J. E., 1976. Compositional variations in wolframite from the Hamme (Tungsten Queen) mine, North Carolina. USGS Journal of Research, 4, 583-588.

Casadevall, T., and Rye, R. O., 1980. The Tungsten Queen deposit, Hamme district, Vance County, North Carolina: A stable isotope study of a metamorphosed quartz-huebnerite vein:

Economic Geology, v. 75, p. 523-537.

Chaumba, Jeff B.; Reid, Jeffrey C., and Parker, Johnathon C., 2015, Hamme (Tungsten Queen) Mine Tailings, Vance County, North Carolina: Mineral Chemistry of Potentially Recoverable

Huebernite-Wolframite and Sulfide Minerals: Southeastern Geology, v. 51, No. 1, p. 33-49.

Espenshade, G. H., 1947, Tungsten deposits of Vance County, North Carolina, and Mecklenburg County, Virginia: U.S. Geol. Survey Bulletin 948-A, 17p.

Feiss, P.G., Maybin III, A.H., Riggs, S.R. and Grosz, A.E., 1991. Mineral resources of the Carolinas, in J.W. Horton and V.A. Zullo (eds.), The Geology of the Carolinas, Carolina Geological

Society Fiftieth Anniversary Volume, p. 319-345.

Foose, Michael P. and Slack, John F., 1978, Premetamorphic hydrothermal origin of the the Tungsten Queen vein, Hamme district, North Carolina, as indicated by mineral textures and

minor structures: U.S. Geological Survey, Open-file report 78-427, 39 p.

Foose, Michael P., Slack, John F. and Casadevall, T., 1980. Textural and structural evidence for predeformation hydrothermal origin of the Tungsten Queen deposit, Hamme district,

North Carolina: Economic Geology, v. 75, p. 515-522.

Gair, J. E., 1977, Maps and diagrams showing structural control of the Hamme tungsten deposit, Vance County, North Carolina: U.S. Geol. Survey Misc. Geol. Inv. Map 1-1009.

Glenn, L.C.; Burwell, E. B.; Espenshade, G.H.; Kline, M.H., and McKeagney, 1948, Report on the investigation of the Hamme Tungsten District in its relationship to the Buggs Island

Reservoir, Roanoke River, VA-N.C.: Advisory Board to the District Engineer, 28 April 1948, 13 p. plus Appendix providing detailed information on individual veins (19 pages).

Glenn, L.C.; Burwell, E. B.; Espenshade, G.H.; Kline, M.H., and McKeagney, 1948, Interim report on investigations of tungsten deposits in Buggs Island Reservoir, Roanoke River, VA- N.C.,

28 January 1948, 22p. with pocket map showing tungten-bearing veins and proposed flooding area relative to tungsten veins.

Hamme, John V., 1954, Steadily Growing Southeastern Tungsten Production, Mining Engineering, p. 978-982 (describes mill flowchart for mine).

Hecla Mining Company, Letter to Mr. Grover Nicholson from Collen D. Kelly, Environmental Supervisor dated February 26, 1985 (tailings study for Ranchers Exploration &

Development Corporation by Ralph Meyertons, November 15, 1975), contained in State of North Carolina, Department of Environment, Health and Natural Resources,

Division of Solid Waste Management, Superfund Section, report Tungsten Queen Mine NCD 082362989, Phase II, Screening Site Inspection – References dated August 1991

by Greenhorne & O’Mara, Inc.

Parker, John M., 3rd, 1963, Geologic setting of the Hamme Tungsten District, North Carolina and Virginia: U.S. Geological Survey, Bulletin 1122-G, 69p.

MP4-H13-102 +30

Width of field of view ~9mm – Setting 1.0 – brass wire mesh fragments shown

MP4-H13-102 +30 to +40

Width of field of view 4.9mm – Setting 2.5

MP4-H13-102 -40 to +50

Width of field of view 4.9mm – Setting 2.5

MP4-H13-102 -50 to +70

Width of field of view 3.5mm – Setting 3.5

MP4-H13-102 -100 to +140

Width of field of view ~3.5mm – Setting 3.5

MP4-H13-102 -200

Width of field of view ~1.2 mm – 100x petrographic oil immersion – plane polarized light

MP4-H13-102 -200

Width of field of view ~1.2 mm – 100x petrographic oil immersion – cross-polarized light

Binocular- and petrographic examination of different size fractions was used to assess mineral concentrate effectiveness. In this series of size

fractions, iron oxide coats quartz grains at all size fraction ranges. This observation led to the need for leaching in order to remove this impurity,

to improve the concentrate quality. Petrographic oil immersion of grains at -200 mesh revealed that iron oxide coated grains in this fraction also.

Lower magnification binocular examination indicated that some feldspars remained, and identified a brass screen mesh fragment. These

observations resulted in further concentrate floatation and leaching leading to a significantly improved concentrate shown below with its

accompanying ICP-MS analysis.

Gravity

Separation

Magnetic

Separation

Floatation

Leaching

High Purity Quartz (HPQ)

Heavy

(tailings)

Magnetic (iron

minerals)

Non-magnetic (quartz)

Feldspar,

mica, iron

minerals

Impurities

Beneficiation of Hamme tungsten quartz (H13 - concentrate MP-4)Summary of processing methods and procedures used in July 2016. Sample H13 is near the tailings

dam, and among the most distal from tailings discharge from the now abandoned gravity mill.

Gravity Separation

Raw ore was processed through a gold miser to remove heavy minerals (tungsten, fluorite, galena,

etc.) from the sand (quartz). The quartz product was saved and used for subsequent beneficiation

processes to produce the high quality quartz product.

Screening

H13 feed was screened over a 30 mesh sieve. The minus 30 mesh fraction (-30 x 0 mesh) was

advanced to wet magnetic separation to remove magnetic mineral impurities.

Wet Magnetic Separation

The minus 30 mesh material was passed 3 times through the Eriez Wet Magnetic Separator set

at 70 volts. Non-mags were collected for subsequent froth flotation processing.

Froth Flotation

The flotation process followed the following steps:

1. Scrubbed for 5 minutes @~65% solids.

2. De-slimed 3 times over 200 mesh sieve.

3. Conditioning at <3.0 pH with (HH-70) petroleum sulfonate for Iron Float #1.

4. Iron Flotation #1.

5. Conditioning at <3.0 pH with (HH-70) petroleum sulfonate for Iron Float #2.

6. Iron Flotation #2.

7. Conditioning at <3.0 pH with amine for Mica Float #1.

8. Mica Flotation #1.

9. Conditioning at <3.0 pH with amine for Mica Float #2.

10. Mica Flotation #2.

11. Conditioning with HF and amine for Feldspar Float #1.

12. Feldspar Flotation #1.

13. Conditioning with HF and amine for Feldspar Float #2.

14. Feldspar Flotation #2.

Note: All reagents used, except collector HM-70, were 2.5% concentration.

The final quartz product (flotation tailings) was dried and advanced to dry magnetic separation

to remove additional magnetic impurities.

Dry Magnetic Separation

The quartz product from the flotation was passed 3 times over a PermRoll Separator to produce

the 30 x 200-mesh non-magnetic quartz product. This non-magnetic quartz product was

subjected to sink-float procedure (Heavy Liquid Separation) to remove additional heavy minerals.

Leaching

Finally the hiqh quality quartz product was subjected to a proprietary hot

acid leaching procedure to remove additional soluble impurities.

Samples with a weight of about 60 pounds were collected along a paced grid with GPS-controlled

sample stations. Sample collection on 13 June 2013 used a power auger and shovel. Samples were

collected in a 5-gallon plastic pail.

Samples were collected from stations H4-H8, and H13-20 (see Google Earth image for locations).

Water was encountered in most drill holes at a depth of <5 feet.

High purity quartz: Applications, impurity levels, market size, and price

Typical High Purity Quartz (HPQ) applicationsThe main applications for high purity quartz are:

- Semiconductors (fillers and silicon metal),

- High temperature lamp tubing,

- Telecommunications and optics,

- Microelectronics, and

- Solar (panel) silicon industries.

Note 1: HPQ = high purity quartz; Mtpa = million tonne per annum; tonne = metric tons.

Note 2: “High grade” high purity quartz with <30ppm other elements is the standard high purity quartz produced by Unimin Corp.

and TQC at Spruce Pine, North Carolina.

Reference (credit): Silica and High Purity Quartz Information, Verdant Minerals, Ltd.

Location of the Tungsten (Hamme) Queen deposit (modified from Espenshade 1947). (After Chaumba and others, 2015).

Geologic map of the Tungsten (Hamme) Queen deposit area

(modified from Espenshade (1947) and Fosse and others

(1980). (After Chaumba and others, 2015).

Determine if a high purity quartz concentratate could be produced

from the Hamme Tungsten (Tungsten Queen) mine tailings.

Tailings sampling was part of a statewide tailings sampling project by North

Carolina’s Minerals Research Laboratory (MRL), Asheville, N.C., to evaluate

potential resources statewide. The North Carolina Geological Survey (NCGS)

collaborated with MRL to evaluate the Hamme (Tungsten Queen) tailings.

Site layout

The Google Earth (GE) image shows the overall site layout. The red grid lines

on the tailings fan surface show the sample grid established for this study.

Samples 1-3 are from the centerline of the unnumbered red cross (sample

numbers increase from west to east). GE area corresponds to map below.

(Above) - Myertons (1975) conducted a preliminary investigation of the tungsten content of the Tungsten Queen tailings pond. He excavated thirteen pits in the pond using

a backhoe. Samples were taken from each pit for grain size and chemical analyses. The image shows the backhoe pit locations. (Above - Right) Myertons concluded that there

are “...2,038,000 tons of material averaging 0.218% WO3 for a total content of 445,600 STU WO

3. This is classed as a probable reserve rather than ‘proven’ or ‘possible’ reserve.”

The backhoe pits ranged from five- to eight feet deep, and nowhere reached the bottom of the sand according to Myertons. He indicated that “...Pond

material appears to be about thirty feet deep over most of the pond, increasing to forty feet in (sic) narrow zone under the 1970 tailing dam. This implies

that the value of the tungsten that could potentially be recovered depends on recovering -400 mesh-size huebernite and separating it from sericite and

mica according to Myertons.

The approximately two million tons of tailings is significant because with the the current concentrate grade this resource may be economic as a silica

resource. Further work may use GPR, and other seismic techniques, supplemented by vibracore drilling to fully confirm tailings sediment thickness.

.

(Left) - Petrographic examination of the light (<2.9 S.G.) fraction showed iron oxide (Fox) rims

surrounding some quartz grains (100x, plane light, field of view width - 1.2mm). Fox decreases the

quality of the concentrate. Its removal necessitated the more extensive leaching process outlined

here. (Right) - Occasional high specific gravity minerals such as fluorite (shown here) and others

(galena, huebernite) were noted in early concentrates (100x, plane light, field of view width - 1.2mm).

Further concentrate processing was required to remove these impurities also.

(Left) is an enlargement of the tailings area corresponding to Myertons’ two million ton

tailings resource. The red square indicates the approximate point where the mill discharged

tailings. The tailings and bedrock profile (above) provide some estimate of tailings thick-

ness.

Tungsten (Hamme)

Queen deposit.

James A. Bailey permitted access to the site for this study.

(Left of this column) Final MP-4 quartz grain

concentrate viewed using a variable pressure SEM.

The grains in the left most image tend to have

been etched comparatively more deeply (”More

etched grain example”) than those shown in the

right image (”Less etched grain example”) during

the beneficiation process.

(Right of this column) SEM-EDS analysis show no

chemical distinction at the grain-size level.

Deleterious elements such as Al, K, and Fe were

not detected by the EDS (elemental peak postions

shown on spectra).

The carbon peak reflects the mounting medium. The

K peak location is within that of the C peak, but no

K is present (see sprectra and analyses - to right).

More etched grain example Less etched grain example

FluoriteFox rims

North Carolina Geological Survey - Open-file report 2017-01